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v <br />0 <br />3 <br />v <br />m <br />Forest Lake <br />0 <br />0 <br />G) <br />� <br />O <br />G <br />T <br />0 <br />J <br />O <br />z <br />O <br />X <br />180TFL SF _—_ _—__—__—__—__ <br />180T'H-.`)�N__—__—__—_ _—__—__—__—_ 1'fl OTH RST� - <br />d <br />v <br />N <br />177 TH ST 1 '7TH ST N c <br />N c I <br />o <br />-* ._ ,. 'L176T S N <br />¢ I_ <br />a <br />G <br />BOTH ST E OF <br />i <br />a <br />i <br />� <br />z,•. <br />> I <br />M <br />!6 <br />Z <br />a <br />Y I <br />a <br />44 <br />- <br />• y1 x� w� <br />158TH <br />159TH <br />ST N .�i <br />H�Fy\S Poe PKLNYN 0��� 15nH 8T N - •, 0O <br />1H STN A�_ <br />-J �. �' <br />i <br />155TH,ST <br />r <br />w 61 <br />i <br />i <br />Q <br />z I Or <br />w <br />a '1 <br />149T H - <br />x <br />FR O 1 8TH ST y <br />MAIN ST s ^ <br />• <br />ENCHMAN <br />1szND sT <br />_ i <br />+y. <br />4 a -- <br />'t <br />11711 <br />147TH ST <br />RN w- <br />J\O.�ORPATy FREN HMANRD_ <br />5 <br />W <br />W <br />0 I <br />ti <br />O <br />1pb <br />�� G) 2 <br />_ <br />� w� -- -w <br />w <br />CEDAR S S <br />Z <br />e <br />�� <br />T ♦ <br />Yr <br />T S N4oT. ST N_ z <br />� 4✓ .. icy, C. ���^� _ <br />k 1 TH STN <br />- <br />STN <br />136THajP <br />Q <br />O <br />V <br />z <br />1N ST N <br />z <br />Z. 132N0 ST N �"y �R <br />a _ c NK-%. <br />a _'Y <br />130TH ST N u' a j O-.-OTH STN N KE <br />'Rv k ■■■ YSTONH <br />D <br />u , z <br />N <br />' <br />�, z <br />2 <br />> <br />m G C <br />m < <br />W L <br />a u <br />TH .ST N <br />12 126TH 9 STN41 <br />W Po <br />z <br />o 0 2 ► I <br />is •. .. _+. i <br />2 <br />Y <br />122ND STN <br />> z <br />21ST STN <br />Anoka <br />Q <br />�� <br />-- -- -- --- <br />Ramsey <br />1zoT�s�-N --- <br />� � m T F <br />C,92O <br />_—___1zoTrF STN -- z. <br />------------•----------- <br />F 3U�YP g19TH ST N <br />?� O �`S<F 2 118TH N <br />W <br />2 K u <br />vEN ST <br />j <br />z W <br />1 <br />L7 O1 �o r" IvrH Sl N <br />m� <br /><. <br />O <br />y O <br />o 0 <br />x A -These soils have high infiltration rates even when thoroughly wetted. <br />These soils consist chiefly of deep, well drained to excessively drained <br />Z <br />Z sands and gravel. These soils haves high rate of water transmission, <br />therefore resulting in a low runoff potential. <br />B- These soils have moderate infiltration rates. These soils consist of <br />deep moderately well to well drained soils with moderately fine to <br />moderately coarse textures. <br />C <br />Grant C -These sots have slow infiltration rates. These soils typloaly consist <br />of clayey gravel or clayey sand. <br />Legend <br />D -These soils have very slow infiltration rates. These soils are are <br />typically clay soils wth high swelling potential at or near the surface <br />or shallow soils over nearly impervious material. <br />Lakes <br />q B/D <br />- <br />Hydrologic <br />Soil Group A/ D C <br />Urban - These soils have been greatly affected by development <br />and are frequency corrected, cut, and filled, grouting in variable <br />runoff rates and a poor environment for plant growth. <br />Urban <br />BC/D <br />Dual Soil Groups - Adequately drained soils when <br />wet are assigned to dual hydrologic soil groups (ArD, BID, <br />and CID) based on their saturated hydraulicconductivity and <br />the water table depth when drained. <br />Oe <br />CITY OF— <br />0 0.25 0.5 Miles <br />Water Resource FIGURE 2: Hydrologic Soils and Infiltration I I A <br />M A N A G [ M [ N i F [ f,5. N 2018 <br />Source: Natural Resources Conservation Service, 2009 <br />